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Adding Vectors, Rules ! When two vectors are
added, the sum is independent of the order of the addition. ! This is the Commutative
Law of Addition !
Adding Vectors, Rules cont. ! When adding three or more vectors, their sum is
independent of the way in which the individual vectors are grouped ! This is called the Associative Property of Addition
!
Adding Vectors, Rules final
! When adding vectors, all of the vectors must have the same units
! All of the vectors must be of the same type of quantity ! For example, you cannot add a displacement to a
velocity
Negative of a Vector ! The negative of a vector is defined as the
vector that, when added to the original vector, gives a resultant of zero ! Represented as !
! The negative of the vector will have the same magnitude, but point in the opposite direction
Subtracting Vectors ! Special case of vector
addition ! If , then use ! Continue with standard
vector addition procedure
Subtracting Vectors, Method 2 ! Another way to look at
subtraction is to find the vector that, added to the second vector gives you the first vector
! ! As shown, the resultant
vector points from the tip of the second to the tip of the first
Multiplying or Dividing a Vector by a Scalar ! The result of the multiplication or division of a vector
by a scalar is a vector ! The magnitude of the vector is multiplied or divided
by the scalar ! If the scalar is positive, the direction of the result is
the same as of the original vector ! If the scalar is negative, the direction of the result is
opposite that of the original vector
Component Method of Adding Vectors
! Graphical addition is not recommended when ! High accuracy is required ! If you have a three-dimensional problem
! Component method is an alternative method ! It uses projections of vectors along coordinate
axes
Components of a Vector, Introduction ! A component is a
projection of a vector along an axis ! Any vector can be
completely described by its components
! It is useful to use rectangular components ! These are the projections
of the vector along the x- and y-axes
Vector Component Terminology
! are the component vectors of ! They are vectors and follow all the rules for
vectors ! Ax and Ay are scalars, and will be referred to
as the components of
Components of a Vector ! Assume you are given
a vector ! It can be expressed in
terms of two other vectors, and
! These three vectors form a right triangle
!
Components of a Vector, 2
! The y-component is moved to the end of the x-component
! This is due to the fact that any vector can be moved parallel to itself without being affected ! This completes the
triangle
Components of a Vector, 3 ! The x-component of a vector is the projection along
the x-axis
! The y-component of a vector is the projection along the y-axis
! This assumes the angle θ is measured with respect to the x-axis ! If not, do not use these equations, use the sides of the
triangle directly
Components of a Vector, 4 ! The components are the legs of the right triangle
whose hypotenuse is the length of A
! May still have to find θ with respect to the positive x-axis
Components of a Vector, final ! The components can
be positive or negative and will have the same units as the original vector
! The signs of the components will depend on the angle
Unit Vectors
! A unit vector is a dimensionless vector with a magnitude of exactly 1.
! Unit vectors are used to specify a direction and have no other physical significance
Unit Vectors, cont. ! The symbols
represent unit vectors ! They form a set of
mutually perpendicular vectors in a right-handed coordinate system
! Remember,
Viewing a Vector and Its Projections ! Rotate the axes for
various views ! Study the projection of
a vector on various planes ! x, y ! x, z ! y, z
Unit Vectors in Vector Notation ! Ax is the same as Ax
and Ay is the same as Ay etc.
! The complete vector can be expressed as
Adding Vectors Using Unit Vectors
! Using ! Then
! and so Rx = Ax + Bx and Ry = Ay + By
Adding Vectors with Unit Vectors ! Note the relationships
among the components of the resultant and the components of the original vectors
! Rx = Ax + Bx ! Ry = Ay + By
Three-Dimensional Extension
! Using ! Then
! and so Rx= Ax+Bx, Ry= Ay+By, and Rz =Ax+Bz
Example 3.5 – Taking a Hike ! A hiker begins a trip by first walking 25.0 km
southeast from her car. She stops and sets up her tent for the night. On the second day, she walks 40.0 km in a direction 60.0° north of east, at which point she discovers a forest ranger’s tower.
Example 3.5 ! (A) Determine the components
of the hiker’s displacement for each day.
Solution: We conceptualize the problem by drawing a sketch as in the figure above. If we denote the displacement vectors on the first and second days by and respectively, and use the car as the origin of coordinates, we obtain the vectors shown in the figure. Drawing the resultant , we can now categorize this problem as an addition of two vectors.
Example 3.5 ! We will analyze this
problem by using our new knowledge of vector components. Displacement has a magnitude of 25.0 km and is directed 45.0° below the positive x axis.
From Equations 3.8 and 3.9, its components are:
The negative value of Ay indicates that the hiker walks in the negative y direction on the first day. The signs of Ax and Ay also are evident from the figure above.
Example 3.5 ! The second
displacement has a magnitude of 40.0 km and is 60.0° north of east.
Its components are:
Example 3.5 ! (B) Determine the
components of the hiker’s resultant displacement for the trip. Find an expression for in terms of unit vectors.
Solution: The resultant displacement for the trip has components given by Equation 3.15:
Rx = Ax + Bx = 17.7 km + 20.0 km = 37.7 km
Ry = Ay + By = -17.7 km + 34.6 km = 16.9 km
In unit-vector form, we can write the total displacement as
Example 3.5 ! Using Equations 3.16 and
3.17, we find that the resultant vector has a magnitude of 41.3 km and is directed 24.1° north of east.
Let us finalize. The units of are km, which is reasonable for a displacement. Looking at the graphical representation in the figure above, we estimate that the final position of the hiker is at about (38 km, 17 km) which is consistent with the components of in our final result. Also, both components of are positive, putting the final position in the first quadrant of the coordinate system, which is also consistent with the figure.
Motion in Two Dimensions ! Using + or – signs is not always sufficient to fully
describe motion in more than one dimension ! Vectors can be used to more fully describe motion ! Will look at vector nature of quantities in more detail
! Still interested in displacement, velocity, and acceleration
! Will serve as the basis of multiple types of motion in future chapters
Position and Displacement ! The position of an
object is described by its position vector,
! The displacement of the object is defined as the change in its position
!
General Motion Ideas
! In two- or three-dimensional kinematics, everything is the same as as in one-dimensional motion except that we must now use full vector notation ! Positive and negative signs are no longer
sufficient to determine the direction
Average Velocity ! The average velocity is the ratio of the displacement
to the time interval for the displacement
! The direction of the average velocity is the direction of the displacement vector
! The average velocity between points is independent of the path taken ! This is because it is dependent on the displacement, also
independent of the path
Instantaneous Velocity ! The instantaneous
velocity is the limit of the average velocity as Δt approaches zero
! As the time interval becomes smaller, the direction of the displacement approaches that of the line tangent to the curve
Instantaneous Velocity, cont
! The direction of the instantaneous velocity vector at any point in a particle’s path is along a line tangent to the path at that point and in the direction of motion
! The magnitude of the instantaneous velocity vector is the speed ! The speed is a scalar quantity
Average Acceleration
! The average acceleration of a particle as it moves is defined as the change in the instantaneous velocity vector divided by the time interval during which that change occurs.
Average Acceleration, cont ! As a particle moves,
the direction of the change in velocity is found by vector subtraction
! The average acceleration is a vector quantity directed along
Instantaneous Acceleration
! The instantaneous acceleration is the limiting value of the ratio as Δt approaches zero
! The instantaneous equals the derivative of the velocity vector with respect to time
Producing An Acceleration
! Various changes in a particle’s motion may produce an acceleration ! The magnitude of the velocity vector may change ! The direction of the velocity vector may change
! Even if the magnitude remains constant ! Both may change simultaneously
Kinematic Equations for Two-Dimensional Motion ! When the two-dimensional motion has a constant
acceleration, a series of equations can be developed that describe the motion
! These equations will be similar to those of one-dimensional kinematics
! Motion in two dimensions can be modeled as two independent motions in each of the two perpendicular directions associated with the x and y axes ! Any influence in the y direction does not affect the motion
in the x direction
Kinematic Equations, 2
! Position vector for a particle moving in the xy plane
! The velocity vector can be found from the position vector
! Since acceleration is constant, we can also find an expression for the velocity as a function of time:
Kinematic Equations, 3
! The position vector can also be expressed as a function of time: ! ! This indicates that the position vector is the sum
of three other vectors: ! The initial position vector ! The displacement resulting from the initial velocity ! The displacement resulting from the acceleration
Kinematic Equations, Graphical Representation of Final Velocity
! The velocity vector can be represented by its components
! is generally not along the direction of either or
Kinematic Equations, Graphical Representation of Final Position
! The vector representation of the position vector
! is generally not along the same direction as or as
! and are generally not in the same direction
Graphical Representation Summary ! Various starting positions and initial velocities
can be chosen ! Note the relationships between changes made
in either the position or velocity and the resulting effect on the other